CHAPTER I.

[Illustration: _Fig. 1._

The Solar System.]

METEORIC ASTRONOMY:

A TREATISE

ON

SHOOTING-STARS, FIRE-BALLS,

AND

AEROLITES.

BY

DANIEL KIRKWOOD, LL.D.

PROFESSOR OF MATHEMATICS IN WASHINGTON AND JEFFERSON COLLEGE.

[Illustration]

PHILADELPHIA:

J. B. LIPPINCOTT & CO.

1867.

Entered, according to Act of Congress, in the year 1867, by

DANIEL KIRKWOOD, LL.D.,

In the Clerk's Office of the District Court of the United States

for the Western District of Pennsylvania.

PREFACE.

Aristotle and other ancient writers regarded comets as meteors

generated in the atmosphere. This opinion was generally accepted, even

by the learned, until the observations of Tycho, near the close of the

sixteenth century, showed those mysterious objects to be more distant

than the moon, thus raising them to the dignity of _celestial_ bodies.

An achievement somewhat similar, and certainly no less interesting,

was reserved for the astronomers of the _nineteenth_ century. This was

the great discovery that _shooting-stars, fire-balls, and meteoric

stones, are, like comets, cosmical bodies moving in conic sections

about the sun_. DR. HALLEY was the first to foretell the return of a

comet, and the year 1759 will ever be known in history as that which

witnessed the fulfillment of his prophecy. But in the department of

_meteoric_ astronomy, a similar honor must now be awarded to the late

DR. OLBERS. Soon after the great star-shower of 1833 he inferred from

a comparison of recorded facts that the November display attains

a maximum at intervals of thirty-three or thirty-four years. He

accordingly designated 1866 or 1867 as the time of its probable return;

and the night of November 13th of the former year must always be

memorable as affording the first verification of _his_ prediction. On

that night several thousand meteors were observed in one hour from a

single station. This remarkable display, together with the fact that

another still more brilliant is looked for in November, 1867, has

given meteoric astronomy a more than ordinary degree of interest in

the public mind. To gratify, in some measure, the curiosity which has

been awakened, by presenting in a popular form the principal results of

observation and study in this new field of research, is the main design

of the following work.

The first two chapters contain a popular view of what is known in

regard to the star-showers of August and November, and also of some

other epochs. The third is a description, in chronological order,

of the most important falls of meteoric stones, together with the

phenomena attending their descent. The fourth and following chapters

to the eleventh inclusive, discuss various questions in the theory

of meteors: such, for instance, as the relative number of aerolitic

falls during different parts of the day, and also of the year; the

coexistence of the different forms of meteoric matter in the same

rings; meteoric dust; the stability of the solar system; the doctrine

of a resisting medium; the extent of the atmosphere as indicated by

meteors; the meteoric theory of solar heat; and the phenomena of

variable and temporary stars. The twelfth chapter regards the rings

of Saturn as dense meteoric swarms, and accounts for the principal

interval between them. The thirteenth presents various facts, not

previously noticed, respecting the asteroid zone between Mars and

Jupiter, with suggestions concerning their cause or explanation.

As the nebular hypothesis furnishes a plausible account of the origin

of meteoric streams, it seemed desirable to present an intelligible

view of that celebrated theory. This accordingly forms the subject of

the closing chapter.

The greater part of the following treatise, it is proper to remark, was

written before the publication (in England) of Dr. Phipson's volume on

"Meteors, Aerolites, and Falling-stars." The author has had that work

before him, however, while completing his manuscript, and has availed

himself of some of the accounts there given of recent phenomena.

CANONSBURG, PA, _May, 1867_.

CONTENTS.

PAGE

INTRODUCTION 7

CHAPTER I.

The Meteors of November 12th-14th 13

CHAPTER II.

Other Meteoric Rings 26

CHAPTER III.

Aerolites 35

CHAPTER IV.

Conjectures in Regard to Meteoric Epochs 50

CHAPTER V.

Geographical Distribution of Meteoric Stones--Do

Aerolitic Falls occur more frequently by Day than by

Night?--Do Meteorites, Bolides, and the matter of ordinary

Shooting-stars, coexist in the same Rings? 56

CHAPTER VI.

Phenomena supposed to be Meteoric--Meteoric Dust--Dark Days 65

CHAPTER VII.

Researches of Reichenbach--Theory of Meteors--Stability of

the Solar System--Doctrine of a Resisting Medium 74

CHAPTER VIII.

Does the Number of Aerolitic Falls vary with the Earth's

Distance from the Sun?--Relative Numbers observed in the

Forenoon and Afternoon--Extent of the Atmosphere as indicated

by Meteors 79

CHAPTER IX.

The Meteoric Theory of Solar Heat 84

CHAPTER X.

Will the Meteoric Theory account for the Phenomena of

Variable and Temporary Stars? 92

CHAPTER XI.

The Lunar and Solar Theories of the Origin of Aerolites 96

CHAPTER XII.

The Rings of Saturn 102

CHAPTER XIII.

The Asteroid Ring between Mars and Jupiter 105

CHAPTER XIV.

Origin of Meteors--The Nebular Hypothesis 112

APPENDIX 123

INTRODUCTION.

A GENERAL VIEW OF THE SOLAR SYSTEM.

THE SOLAR SYSTEM consists of the sun, together with the planets and

comets which revolve around him as the center of their motions. The sun

is the great controlling orb of this system, and the source of light

and heat to its various members. Its magnitude is one million four

hundred thousand times greater than that of the earth, and it contains

more than seven hundred times as much matter as all the planets put

together.

MERCURY is the nearest planet to the sun; its mean distance being about

thirty-seven millions of miles. Its diameter is about three thousand

miles, and it completes its orbital revolution in 88 days.

VENUS, the next member of the system, is sometimes our morning and

sometimes our evening star. Its magnitude is almost exactly the same as

that of the earth. It revolves round the sun in 225 days.

THE EARTH is the third planet from the sun in the order of distance;

the radius of its orbit being about ninety-five millions of miles. It

is attended by one satellite--the moon--the diameter of which is 2160

miles.

MARS is the first planet exterior to the earth's orbit. It is

considerably smaller than the earth, and has no satellite. It revolves

round the sun in 687 days.

THE ASTEROIDS.--Since the commencement of the present century a

remarkable zone of telescopic planets has been discovered immediately

exterior to the orbit of Mars. These bodies are extremely small; some

of them probably containing less matter than the largest mountains on

the earth's surface. More than ninety members of the group are known at

present, and the number is annually increasing.

JUPITER, the first planet exterior to the asteroids, is nearly five

hundred millions of miles from the sun, and revolves round him in a

little less than twelve years. This planet is ninety thousand miles in

diameter and contains more than twice as much matter as all the other

planets, primary and secondary, put together. Jupiter is attended by

four moons or satellites.

SATURN is the seventh planet in the order of distance--counting the

asteroids as one. Its orbit is about four hundred millions of miles

beyond that of Jupiter. This planet is attended by eight satellites,

and is surrounded by three broad, flat rings. Saturn is seventy-six

thousand miles in diameter, and its mass or quantity of matter is more

than twice that of all the other planets except Jupiter.

URANUS is at double the distance of Saturn, or nineteen times that

of the earth. Its diameter is about thirty-five thousand miles, and

its period of revolution, eighty-four years. It is attended by four

satellites.

NEPTUNE is the most remote known member of the system; its distance

being nearly three thousand millions of miles. It is somewhat larger

than Uranus; has certainly one satellite, and probably several more.

Its period is about one hundred and sixty-five years. A cannon-ball

flying at the rate of five hundred miles per hour would not reach the

orbit of Neptune from the sun in less than six hundred and eighty years.

These planets all move round the sun in the same direction--from west

to east. Their motions are nearly circular, and also nearly in the same

plane. Their orbits, except that of Neptune, are represented in the

frontispiece. It is proper to remark, however, that all representations

of the solar system by maps and planetariums must give an exceedingly

erroneous view either of the magnitudes or distances of its various

members. If the earth, for instance, be denoted by a ball half an

inch in diameter, the diameter of the sun, according to the same

scale (sixteen thousand miles to the inch), will be between four and

five feet; that of the earth's orbit, about one thousand feet; while

that of Neptune's orbit will be nearly six miles. To give an accurate

representation of the solar system at a single view is therefore

plainly impracticable.

COMETS.--The number of comets belonging to our system is unknown. The

appearance of more than seven hundred has been recorded, and of this

number, the elements of about two hundred have been computed. They move

in very eccentric orbits--some, perhaps, in parabolas or hyperbolas.

THE ZODIACAL LIGHT is a term first applied by Dominic Cassini, in

1683, to a faint nebulous aurora, somewhat resembling the milky-way,

apparently of a conical or lenticular form, having its base toward

the sun, and its axis nearly in the direction of the ecliptic. The

most favorable time for observing it is when its axis is most nearly

perpendicular to the horizon. This, in our latitudes, occurs in March

for the evening, and in October for the morning. The angular distance

of its vertex from the sun is frequently seventy or eighty degrees,

while sometimes, though rarely (except within the tropics), it exceeds

even one hundred degrees.

The zodiacal light is probably identical with the meteor called

_trabes_ by _Pliny_ and _Seneca_. It was noticed in the latter part

of the sixteenth century by Tycho Brahé, who "considered it to be an

abnormal spring-evening twilight." It was described by Descartes

about the year 1630, and again by Childrey in 1661. The first accurate

description of the phenomenon was given, however, by Cassini. This

astronomer supposed the appearance to be produced by the blended

light of an innumerable multitude of extremely small planetary bodies

revolving in a ring about the sun. The appearance of the phenomenon as

seen in this country is represented in Fig. 2.

[Illustration: Fig. 2.]

For general readers it may not be improper to premise the following

explanations:

Meteors are of two kinds, _cosmical_ and _terrestrial_: the former

traverse the interplanetary spaces; the latter originate in the earth's

atmosphere.

_Bolides_ is a general name for meteoric fire-balls of greater

magnitude than shooting-stars.

The _period_ of a planet, comet, or meteor is the time which it

occupies in completing one orbital revolution.

The motion of a heavenly body is said to be _direct_ when it is from

west to east; and _retrograde_ when it is from east to west.

_Encke's Hypothesis of a Resisting Medium._--The time occupied by

Encke's comet in completing its revolution about the sun is becoming

less and less at each successive return. Professor Encke explains

this fact by supposing the interplanetary spaces to be filled with an

extremely rare fluid, the resistance of which to the cometary motion

produces the observed contraction of the orbit.

METEORIC ASTRONOMY.

CHAPTER I.

SHOOTING-STARS.

I. The Meteors of November 12th-14th.

Although shooting-stars have doubtless been observed in all ages of the

world, they have never, until recently, attracted the special attention

of scientific men. The first exact observations of the phenomena were

undertaken, about the close of the last century, by Messrs. Brandes and

Benzenberg. The importance, however, of this new department of research

was not generally recognized till after the brilliant meteoric display

of November 13th, 1833. This shower of fire can never be forgotten

by those who witnessed it.[1] The display was observed from the West

Indies to British America, and from 60° to 100° west longitude from

Greenwich. Captain Hammond, of the ship Restitution, had just arrived

at Salem, Massachusetts, where he observed the phenomenon from midnight

till daylight. He noticed with astonishment that precisely one year

before, viz., on the 13th of November, 1832, he had observed a similar

appearance (although the meteors were less numerous) at Mocha, in

Arabia. It was soon found, moreover, as a further and most remarkable

coincidence, that an extraordinary fall of meteors had been witnessed

on the 12th of November, 1799. This was seen and described by Andrew

Ellicott, Esq., who was then at sea near Cape Florida. It was also

observed in Cumana, South America, by Humboldt, who states that it

was "simultaneously seen in the new continent, from the equator to

New Herrnhut, in Greenland (lat. 64° 14´), and between 46° and 82°

longitude."

This wonderful correspondence of dates excited a very lively interest

throughout the scientific world. It was inferred that a recurrence

of the phenomenon might be expected, and accordingly arrangements

were made for systematic observations on the 12th, 13th, and 14th of

November. The periodicity of the shower was thus, in a very short

time, placed wholly beyond question. The examination of old historical

records led to the discovery of at least 12 appearances of the November

shower previous to the great fall of 1833. The descriptions of these

phenomena will be found collected in an interesting article by Prof.

H. A. Newton, in the _American Journal of Science and Arts_, for May,

1864. They occurred in the years 902, 931, 934, 1002, 1101, 1202,

1366, 1533, 1602, 1698, 1799, and 1832. Besides these 12 enumerated by

Professor Newton as "the predecessors of the great exhibition on the

morning of November 13th, 1833," we find 6 others, less distinctly

marked, in the catalogue of M. Quetelet.[2] These were in the years

1787, 1818, 1822, 1823, 1828, and 1831. From 1883 to 1849, inclusive,

Quetelet's catalogue indicates 11 partial returns of the November

shower; making in all, up to the latter date, 29. In 1835, November

13th, a straw roof was set on fire by a meteoric fire-ball, in the

department de l'Aine, France. On the 12th of November, 1837, "at 8

o'clock in the evening, the attention of observers in various parts

of Great Britain was directed to a bright luminous body, apparently

proceeding from the North, which, after making a rapid descent, in the

manner of a rocket, suddenly burst, and scattering its particles into

various beautiful forms, vanished in the atmosphere. This was succeeded

by others all similar to the first, both in shape and the manner of its

ultimate disappearance. The whole display terminated at ten o'clock,

when dark clouds, which continued up till a late hour, overspread the

earth, preventing any further observations."--_Milner's Gallery of

Nature_, p. 142.

In 1838, November 12th-13th, meteors were observed in unusual numbers

at Vienna. One of extraordinary brilliancy, having an apparent

magnitude equal to that of the full moon, was seen near Cherburg.

On several other returns of the November epoch the number of meteors

observed has been greater than on ordinary nights; the distinctly

marked exhibitions, however, up to 1866, have all been enumerated.

THE SHOWER OF NOVEMBER 14, 1866.

The fact that all great displays of the November meteors have

taken place at intervals of thirty-three or thirty-four years, or

some multiple of that period, had led to a general expectation of

a brilliant shower in 1866. In this country, however, the public

curiosity was much disappointed. The numbers seen were greater than

on ordinary nights, but not such as would have attracted any special

attention. The greatest number recorded at any one station was seen at

New Haven, by Prof. Newton. On the night of the 12th, 694 were counted

in five hours and twenty minutes, and on the following night, 881

in five hours. This was about six times the ordinary number. A more

brilliant display was, however, witnessed in Europe. Meteors began

to appear in unusual frequency about eleven o'clock on the night of

the 13th, and continued to increase with great rapidity for more than

two hours; the maximum being reached a little after one o'clock. The

Edinburgh _Scotsman_, of November 14th, contains a highly interesting

description of the phenomenon as observed at that city. "Standing on

the Calton Hill, and looking westward," the editor remarks,--"with

the Observatory shutting out the lights of Prince's Street--it was

easy for the eye to delude the imagination into fancying some distant

enemy bombarding Edinburgh Castle from long range; and the occasional

cessation of the shower for a few seconds, only to break out again with

more numerous and more brilliant drops of fire, served to countenance

this fancy. Again, turning eastward, it was possible now and then to

catch broken glimpses of the train of one of the meteors through the

grim dark pillars of that ruin of most successful manufacture, the

National Monument; and in fact from no point in or out of the city was

it possible to watch the strange rain of stars, pervading as it did all

points of the heavens, without pleased interest, and a kindling of the

imagination, and often a touch of deeper feeling that bordered on awe.

The spectacle, of which the loftiest and most elaborate description

could but be at the best imperfect--which truly should have been seen

to be imagined--will not soon pass from the memories of those to whose

minds were last night presented the mysterious activities and boundless

fecundities of that universe of the heavens, the very unchangeableness

of whose beauty has to many made it monotonous and of no interest."

The appearance of the phenomenon, as witnessed at London, is minutely

described in the _Times_ of November 15th. The shower occurred chiefly

between the hours of twelve and two. About one o'clock a single

observer counted 200 in two minutes. The whole number seen at Greenwich

was 8485. The shower was also observed in different countries on the

continent.

_The Meteors of 1866 compared with those of former Displays._

The star shower of 1866 was much inferior to those of 1799 and

1833.[3] With these exceptions, however, it has, perhaps, been

scarcely surpassed during the last 500 years. Historians represent the

meteors of 902 as innumerable, and as moving like rain in all possible

directions.[4] The exhibition of 1202 was no less magnificent. The

stars, it is said, were seen to dash against each other like swarms of

locusts; the phenomenon lasting till daybreak.[5] The shower of 1366

is thus described in a Portuguese chronicle, quoted by Humboldt: "In

the year 1366, twenty-two days of the month of October being past,

three months before the death of the king, Dom Pedro (of Portugal),

there was in the heavens a movement of stars, such as men never before

saw or heard of. At midnight, and for some time after, all the stars

moved from the east to the west; and after being collected together,

they began to move, some in one direction, and others in another.

And afterward they fell from the sky in such numbers, and so thickly

together, that as they descended low in the air, they seemed large and

fiery, and the sky and the air seemed to be in flames, and even the

earth appeared as if ready to take fire. That portion of the sky where

there were no stars, seemed to be divided into many parts, and this

lasted for a long time."

The following is Humboldt's description of the shower of 1799, as

witnessed by himself and Bonpland, in Cumana, South America: "From half

after two, the most extraordinary luminous meteors were seen toward the

east.... Thousands of bolides and falling stars succeeded each other

during four hours. They filled a space in the sky extending from the

true east 30° toward the north and south. In an amplitude of 60° the

meteors were seen to rise above the horizon at E. N. E. and at E.,

describe arcs more or less extended, and fall toward the south, after

having followed the direction of the meridian. Some of them attained a

height of 40°, and all exceeded 25° or 30°.... Mr. Bonpland relates,

that from the beginning of the phenomenon there was not a space in

the firmament equal in extent to three diameters of the moon, that

was not filled at every instant with bolides and falling-stars....

The Guaiqueries in the Indian suburb came out and asserted that the

firework had begun at one o'clock.... The phenomenon ceased by degrees

after four o'clock, and the bolides and falling-stars became less

frequent; but we still distinguished some toward the northeast a

quarter of an hour after sunrise."

DISCUSSION OF THE PHENOMENA.

Since the memorable display of November 13th, 1833, the phenomena of

shooting-stars have been observed and discussed by Brandes, Benzenberg,

Olbers, Saigey, Heis, Olmsted, Herrick, Twining, Newton, Greg, and many

others. In the elaborate paper of Professor Olmsted, it was shown that

the meteors had their origin at a distance of more than 2000 miles

from the earth's surface; that their paths diverged from a common point

near the star _Gamma Leonis_; that in a number of instances they became

visible about 80 miles from the earth's surface; that their velocity

was comparable to that of the earth in its orbit; and that in some

cases their extinction occurred at an elevation of 30 miles. It was

inferred, moreover, that they consisted of combustible matter which

took fire and was consumed in passing through the atmosphere; that this

matter was derived from a nebulous body revolving round the sun in an

elliptical orbit, but little inclined to the plane of the ecliptic;

that its aphelion was near that point of the earth's orbit through

which we annually pass about the 13th of November--the perihelion being

a little within the orbit of Mercury; and finally that its period was

about one-half that of the earth. Dr. Olmsted subsequently modified his

theory, having been led by further observations to regard the zodiacal

light as the nebulous body from which the shooting-stars are derived.

The latter hypothesis was also adopted by the celebrated Biot.

The fact that the position of the radiant point does not change with

the earth's rotation, places the cosmical origin of the meteors wholly

beyond question. The theory of a closed ring of nebulous matter

revolving round the sun in an elliptical orbit which intersects that

of the earth, affords a simple and satisfactory explanation of the

phenomena. This theory was adopted by Humboldt, Arago, and others,

shortly after the occurrence of the meteoric shower of 1833. That the

body which furnishes the material of these meteors moves in a closed

or elliptical orbit is evident from the periodicity of the shower. It

is also manifest from the partial recurrence of the phenomenon from

year to year, that the matter is diffused around the orbit; while the

extraordinary falls of 1833, 1799, 1366, and 1202, prove the diffusion

to be far from uniform.

ELEMENTS OF THE ORBIT.

Future observations, it may be hoped, will ultimately lead to an

accurate determination of the elements of this ring: many years,

however, will probably elapse before all the circumstances of its

motion can be satisfactorily known. Professor Newton, of Yale College,

has led the way in an able discussion of the observations.[6] He has

shown that the different parts of the ring are, in all probability, of

very unequal density; that the motion is retrograde; and that the time,

during which the meteors complete a revolution about the sun, must be

limited to one of five accurately determined periods, viz.: 180·05

days, 185·54 days, 354·62 days, 376·5 days, or 33·25 years. He makes

the inclination of the ring to the ecliptic about 17°. The five periods

specified, he remarks, "are not all equally probable. Some of the

members of the group which visited us last November [1863] gave us the

means of locating approximately the central point of the region from

which the paths diverge. Mr. G. A. Nolen has, by graphical processes

specially devised for the purpose, found its longitude to be 142°, and

its latitude 8° 30´. This longitude is very nearly that of the point

in the ecliptic toward which the earth is moving. Hence the point

from which the absolute motion of the bodies is directed (being in a

great circle through the other two points) has the same longitude. The

absolute motion of each meteor, then, is directed very nearly at right

angles to a line from it to the sun, the deviation being probably not

more than two or three degrees.

"Now, if in one year the group make 2 ± 1/33·25 revolutions, there is

only a small portion of the orbit near the aphelion which fulfills the

above condition. In like manner, if the periodic time is 33·25 years,

only a small portion of the orbit near the perihelion fulfills it.

On the other hand, if the annual motion is 1 ± 1/33·25 revolutions,

the required condition is answered through a large part of the orbit.

Inasmuch as no reason appears why the earth should meet a group near

its apsides rather than elsewhere, we must regard it as more probable

that the group makes in one year either 1 + 1/33·25, or 1 - 1/33·25

revolutions."

Professor Newton concludes that the third of the above-mentioned

periods, viz., 354·62 days, combines the greatest amount of probability

of being the true one. We grant the force of the reasons assigned for

its adoption. At least one consideration, however, in favor of the

long period of 33·25 years is by no means destitute of weight: of

nearly 100 known bodies which revolve about the sun in orbits of small

eccentricity, not one has a retrograde motion. Now if this striking

fact has resulted from a general cause, how shall we account for the

backward motion of a meteoric ring, in an orbit almost circular, and

but little inclined to the plane of the ecliptic? In such a case, is

not the preponderance of probability in favor of the longer period?

A revolution in 33·25 years corresponds to an ellipse whose major axis

is 20·6. Consequently the aphelion distance would be somewhat greater

than the mean distance of Uranus. It may also be worthy of note, that

five periods of the ring would be very nearly equal to two of Uranus.

The _Monthly Notices of the Royal Astronomical Society_ for December,

1866, and January, 1867, contain numerous articles on the star shower

of November 13th-14th, 1866. Sir John Herschel carefully observed the

phenomena, and his conclusions in regard to the orbit are confirmatory

of those of Professor Newton. "We are constrained to conclude," he

remarks, "that the true line of direction, in space of each meteor's

flight, lay in a plane at right angles to the earth's radius vector at

the moment; and that therefore, except in the improbable assumption

that the meteor was at that moment _in perihelio_ or _in aphelio_, its

orbit would not deviate greatly from the circular form." The question

is one to be decided by observation, and the only meteor whose track

and time of flight seem to have been well observed, is that described

by Professor Newton in _Silliman's Journal_ for January, 1867, p. 86.

The velocity in this case, if the estimated time of flight was nearly

correct, was _inconsistent with the theory of a circular orbit_.

It is also worthy of notice that Dr. Oppolzer's elements of the first

comet of 1866 resemble, in a remarkable manner, those of the meteoric

ring, supposing the latter to have a period of about 33-1/4 years.

Schiaparelli's elements of the November ring, and Oppolzer's elements

of the comet of 1866, are as follows:

November Comet of

Meteors. 1866.

Longitude of perihelion 56° 25´ 60° 28´

Longitude of ascending node. 231 28 231 26

Inclination 17 44 17 18

Perihelion distance 0·9873 0·9765

Eccentricity 0·9046 0·9054

Semi-axis major 10·3400 10·3240

Period, in years 33·2500 33·1760

Motion Retrograde. Retrograde.

It seems very improbable that these coincidences should be accidental.

Leverrier and other astronomers have found elements of the meteoric

orbit agreeing closely with those given by Schiaparelli. Should the

identity of the orbits be fully confirmed, it will follow that the

comet of 1866 _is a very large meteor_ of the November stream.

The researches of Professor C. Bruhns, of Leipzig, in regard to this

group of meteors afford a probable explanation of the division of

Biela's comet--a phenomenon which has greatly perplexed astronomers for

the last twenty years. Adopting the period of 33-1/4 years, Professor

Bruhns finds that the comet passed extremely near, and probably

_through_ the meteoric ring near the last of December, 1845. It is easy

to perceive that such a collision might produce the separation soon

afterward observed.

As the comet of Biela makes three revolutions in twenty years, it was

again at this intersection, or approximate intersection of orbits about

the end of 1865. But although the comet's position, with respect to

the earth, was the same as in 1845-6, and although astronomers watched

eagerly for its appearance, their search was unsuccessful. In short,

_the comet is lost_. The denser portion of the meteoric stream was then

approaching its perihelion. A portion of the arc had even passed that

point, as a meteoric shower was observed at Greenwich on the 13th of

November, 1865.[7] The motion of the meteoric stream is retrograde;

that of the comet, direct. Did the latter plunge into the former, and

was its non appearance the result of such collision and entanglement?

[Illustration: Fig. 3.

_Probable Orbit of the November Meteors._]

Meteoric astronomy: A treatise on shooting-stars, fire-balls, and aerolites · 第 1 / 14 章